Abstract
AbstractThe Xiaojiang fault zone (XJFZ) is an important part of the Xianshuihe-Xiaojiang fault system, acting as the eastern boundary of the Chuan-Dian block on the southeastern margin of the Tibetan Plateau and accommodating the lateral extrusion of the block. The faulting activity and paleoseismic history on the southern segment of the XJFZ remain poorly understood. Here, trench excavations and radiocarbon dating revealed that four recent surface-rupturing paleoearthquakes have occurred on the Jianshui fault (JSF) in the southern segment of the XJFZ since ~15370 yr BP. The ages of these events, labeled E4-E1 from oldest to youngest, are limited to the following time ranges: 15360-12755, 10845-6900, 1455-670, and 635-145 yr BP, respectively. The most recent event E1 was most likely the 1606 Jianshui earthquake. These events appear to occur unregularly in time. The time interval between the last two events is 726±235 yr, and the average recurrence interval for all four events is 4589±3132 yr. The deformed strata show that the JSF is characterized kinematically by transtension, which likely respond to the apparent change in the direction of clockwise rotation of the Chuan-Dian block around the eastern Himalayan syntaxis. Combined with the analysis of the neighboring NW-striking faults, our study suggests that the south-southeastward motion of the Chuan-Dian block is likely to be firstly accommodated in part by the right-lateral shear and dip-slip motions of the Qujiang and Shiping faults and continues across the Red River fault zone, then is transmitted southward along the Dien Bien Phu fault. Therefore, the southern segment of the XJFZ plays a dominant role in the tectonic deformation of the southeastern Chuan-Dian block, with a high seismic hazard.
Highlights
The Xiaojiang fault zone (XJFZ) constitutes the continuous Xianshuihe-Xiaojiang left-lateral strike-slip fault system, together with the Xianshuihe fault zone, Anninghe-Zemuhe fault zone, and Daliangshan fault zone (Figure 1(a))
The fault system acts as the eastern boundary of the ChuanDian block on the southeastern margin of the Tibetan Plateau and plays a key role in accommodating the lateral extrusion of the block and clockwise rotation around the eastern Himalayan syntaxis (e.g., [1,2,3,4,5])
Trench excavations and radiocarbon dating revealed that the four most recent surface-rupturing paleoearthquakes on the Jianshui fault (JSF) have occurred since approximately 15370 yr BP
Summary
The Xiaojiang fault zone (XJFZ) constitutes the continuous Xianshuihe-Xiaojiang left-lateral strike-slip fault system, together with the Xianshuihe fault zone, Anninghe-Zemuhe fault zone, and Daliangshan fault zone (Figure 1(a)). The tectonic deformation and seismicity of the XJFZ have been intense since the late Quaternary, and the fault zone forms a vital part of the north-south seismic belt [6,7,8]. The northern segment is located on the northern side of Dongchuan County and is composed of a single fault (Figure 1(a)). The central segment is divided into eastern and western branches that extend from Dongchuan County to Fuxian Lake. The southern segment is located on the southern side of Fuxian Lake and is composed of multiple fault branches to the north of the Jianshui Basin. There is only one fault branch near and to the south of the Jianshui Basin, which is called the Jianshui fault (JSF; Figure 1(a); [12])
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